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33篇 您的检索式:作者名="Gluyas"
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1Distribution Characteristics and Accumulation Model for the Coal-formed Gas Generated from Permo-Carboniferous Coal Measures in Bohai Bay Basin, China: A Review显示文摘Coal-formed gas generated from the Permo-Carboniferous coal measures has become one of the most important targets for deep hydrocarbon exploration in the Bohai Bay Basin,offshore eastern China.However,the proven gas reserves from this source rock remain low to date,and the distribution characteristics and accumulation model for the coal-formed gas are not clear.Here we review the coal-formed gas deposits formed from the Permo-Carboniferous coal measures in the Bohai Bay Basin.The accumulations are scattered,and dominated by middle-small sized gas fields,of which the proven reserves ranging from 0.002 to 149.4×108 m3 with an average of 44.30×108 m3 and a mid-point of 8.16×108 m3.The commercially valuable gas fields are mainly found in the central and southern parts of the basin.Vertically,the coal-formed gas is accumulated at multiple stratigraphic levels from Paleogene to Archaeozoic,among which the Paleogene and PermoCarboniferous are the main reservoir strata.According to the transporting pathway,filling mechanism and the relationship between source rocks and reservoir,the coal-formed gas accumulation model can be defined into three types:'Upward migrated,fault transported gas'accumulation model,'Laterally migrated,sandbody transported gas'accumulation model,and'Downward migrated,sub-source,fracture transported gas'accumulation model.Source rock distribution,thermal evolution and hydrocarbon generation capacity are the fundamental controlling factors for the macro distribution and enrichment of the coal-formed gas.The fault activity and the configuration of fault and caprock control the vertical enrichment pattern.JIANG Youlu HU Hongjin Jon GLUYAS ZHAO Kai 2019Acta Geologica Sinica(English Edition)2019,93,6:4
2How important is carbonate dissolution in buried sandstones:evidences from petrography,porosity,experiments,and geochemical calculations显示文摘Burial dissolution of feldspar and carbonate minerals has been proposed to generate large volumes of secondary pores in subsurface reservoirs. Secondary porosity due to feldspar dissolution is ubiquitous in buried sandstones;however, extensive burial dissolution of carbonate minerals in subsurface sandstones is still debatable. In this paper, we first present four types of typical selective dissolution assemblages of feldspars and carbonate minerals developed in di erent sandstones. Under the constraints of porosity data, water–rock experiments, geochemical calculations of aggressive fluids, diagenetic mass transfer, and a review of publications on mineral dissolution in sandstone reservoirs, we argue that the hypothesis for the creation of significant volumes of secondary porosity by mesodiagenetic carbonate dissolution in subsurface sandstones is in conflict with the limited volume of aggressive fluids in rocks. In addition, no transfer mechanism supports removal of the dissolution products due to the small water volume in the subsurface reservoirs and the low mass concentration gradients in the pore water. Convincing petrographic evidence supports the view that the extensive dissolution of carbonate cements in sandstone rocks is usually associated with a high flux of deep hot fluids provided via fault systems or with meteoric freshwater during the eodiagenesis and telodiagenesis stages. The presumption of extensive mesogenetic dissolution of carbonate cements producing a significant net increase in secondary porosity should be used with careful consideration of the geological background in prediction of sandstone quality.Guang-Hui Yuan Ying-Chang Cao Jon Gluyas Yan-Zhong Wang Ke-Yu Liu Ke-Lai Xi Tian Yang Jian Wang 2019Petroleum Science2019,16,4:4
3The cholinergic system in Alzheimer's disease显示文摘Kasa P Pakonczay Z Gluya K 1997Prog Neurobiol1997,52,:2
4The cholinergic system in Alzheimer's disease显示文摘Kasa P Pakonczay Z Gluya K 1997Prog Neurobiol1997,5,2:1
5Reservoir quality prediction in sandstones and carbonates显示文摘Kupecz J A Gluyas J G Bloch S 1997AAPG Memoir1997,69,:1
6The age of illite cement growth,village fields area,southern north sea:evidence from K-Ar ages and 18O/16O ratios显示文摘 Coleman M L Gluyas J G 1993AAPG Bulletin1993,77,1:1
7Reservoir Quality Prediction in Sandstones and Carbonates显示文摘KUPECZ J A GLUYAS J G BLOCH S 1997AAPG Memoir 691997,,:1
8Prediction of porosity in com pactedsands显示文摘GLUYAS J CADE C A 1997AAPG Memoir 691997,,:1
9Prediction of porosity in compacted sands 显示文摘Gluyas J Cade C A 1997AAPG Memoir1997,69,:1
10Chronic aluminum treatment result in aluminum deposits and affects M1 muscarinic receptors in rat brain 显示文摘Harkany T Lengyel Z Kasa P Gluya K 1996Neurobiology1996,4,12:1
11Reservoir quality prediction in sandstones and carbonates: An overview显示文摘Kupecz J A Gluyas J Bloch S 1997AAPG Memoir1997,69,:1
12The age of illite cement growth, village fields area, southern North Sea: evidence from K-Ar ages and^18O/^16O ratios显示文摘ROBINSON A G COLEMAN M L GLUYAS J G 1993AAPG Bulletin1993,77,:1
13The filling and emptying of the Ula Oilfield:fluid inclusion constraints显示文摘OXTOBY N H MITCHELL A W GLUYAS J G 1995Geological Society Special Publication1995,86,:1
14Prediction of porosity in compacted sands 显示文摘Gluyas J Christopher A C 1998AAPG Memoir1998,69,:1
15Reservoir quality prediction in sandstones and carbonates: an overview 显示文摘Kupecz J A Gluyas J Bloch S 1997AAPG Memoir1997,69,:1
16Modelling and monito- ring of geological carbon storage : A perspective on cross-valida- tion 显示文摘Jiang X Akber Hassan W A Gluyas J 2013Applied Energy2013,112,:1
17Duration of quartz cementation in sand- stones, North Sea and Haltenbankan basins 显示文摘Robinson A Gluyas J 1992Marine and Petroleum Geology1992,9,3:1
18The cholinergic system in Alzheimer's disease显示文摘Kasa P Pakonczay Z Gluya K 1997Prog Neurobiol1997,52,:1
19The cholinergic system in Alzheimer's disease 显示文摘Kasa P Pakonezay Z Gluya K 1997Prog Neurochiol1997,52,:1
20Characteristics of near-fatal asthma in children显示文摘Martin AJ Campbell DA Gluyas PA 1995Pediatr Pulmonol1995,20,1:1
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